US11143790B2ActiveUtilityA1

Modelling geological faults

Assignee: TOTAL SAPriority: Oct 3, 2016Filed: Oct 3, 2016Granted: Oct 12, 2021
Est. expiryOct 3, 2036(~10.2 yrs left)· nominal 20-yr term from priority
G01V 99/005G01V 20/00
33
PatentIndex Score
0
Cited by
6
References
14
Claims

Abstract

To model hydrocarbon reservoirs more accurately, models of a geological volume using a three dimensional grid of cells populated with data from seismic studies are augmented by providing fine-grained stochastic models of the distribution of relays in fault zones and modelling the flow of hydrocarbons taking account the modelled relays.

Claims

exact text as granted — not AI-modified
The invention claimed is: 
     
       1. A method of simulating fluid flow in a geological volume comprising a geological fault, the method comprising:
 generating a three dimensional grid of cells representative of the structure of the geological volume, the cells comprising base cells; 
 classifying a plurality of base cells as fault cells corresponding to the fault in the geological volume; 
 classifying one or more sets of fault cells as relay cell sets corresponding to assumed locations of relays within the fault in the geological volume; 
 generating a three dimensional relay grid of relay sub-cells in the place of each relay cell set, the relay sub-cells of each relay grid being representative of a relay structure within the geological fault and having a finer grid-cell dimension than that of the cells of the relay cell set; 
 determining transmissibilities between the relay sub-cells; 
 determining transmissibilities between the relay cell sets based on the determined transmissibilities between the relay sub-cells, and 
 determining transmissibilities between the base cells based on the determined transmissibilities between the relay sub-cells, wherein the classification of the one or more relay cell sets provides a spatially even distribution of relay cell sets along the direction of the length of the fault. 
 
     
     
       2. The method according to  claim 1 , wherein the classification of the one or more relay cell sets corresponds to a random spatial distribution of relay cell sets along the direction of the length of the fault. 
     
     
       3. The method according to  claim 1 , wherein a poisson point process is employed in order to classify the one or more relay cell sets. 
     
     
       4. The method according to  claim 1 , wherein the number of classified relay cell sets is determined based on the length of the fault represented by the fault cells. 
     
     
       5. The method according to  claim 1 , wherein the fluid flow is simulated over multiple iterations, each new iteration comprising reclassifying one or more sets of cells as relay cell sets. 
     
     
       6. The method according to  claim 1 , wherein one or more relay shape parameters are assigned to the relay cell sets and the calculation of the transmissibilities between the relay sub-cells takes into account the one or more relay shape parameters. 
     
     
       7. The method according to  claim 6 , wherein the one or more relay shape parameters include width, length, and vertical extent of the relay. 
     
     
       8. The method according to  claim 1 , wherein the classifying of the relay cell sets, generation of the relay grid of relay sub-cells and calculation of transmissibilities between relay sub-cells is repeated for each fault identified in the geological volume. 
     
     
       9. The method according to  claim 1 , wherein the one or more sets of cells classified as relay cell sets are base cells. 
     
     
       10. The method according to  claim 1 , wherein:
 the vertical faces of the fault cells are vertically offset from the fault; and
 the fault cells comprise cutted fault cells and non-cutted fault cells, the cutted fault cells having a reduced height as compared to the height of the non-cutted fault cells. 
 
 
     
     
       11. A processing device arranged to implement the method as claimed in  claim 1 . 
     
     
       12. A computer readable medium comprising computer program instructions that when executed on a processor perform the method according to  claim 1 . 
     
     
       13. A method of simulating fluid flow in a geological volume comprising a geological fault, the method comprising:
 generating a three dimensional grid of cells representative of the structure of the geological volume, the cells comprising base cells; 
 classifying a plurality of base cells as fault cells corresponding to the fault in the geological volume; 
 classifying one or more sets of fault cells as relay cell sets corresponding to assumed locations of relays within the fault in the geological volume; 
 generating a three dimensional relay grid of relay sub-cells in the place of each relay cell set, the relay sub-cells of each relay grid being representative of a relay structure within the geological fault and having a finer grid-cell dimension than that of the cells of the relay cell set; 
 determining transmissibilities between the relay sub-cells; 
 determining transmissibilities between the relay cell sets based on the determined transmissibilities between the relay sub-cells, and 
 determining transmissibilities between the base cells based on the determined transmissibilities between the relay sub, wherein the number of classified relay cell sets is determined based on a random distribution. 
 
     
     
       14. A method of simulating fluid flow in a geological volume comprising a geological fault, the method comprising:
 generating a three dimensional grid of cells representative of the structure of the geological volume, the cells comprising base cells; 
 classifying a plurality of base cells as fault cells corresponding to the fault in the geological volume; 
 classifying one or more sets of the fault cells as relay cell sets corresponding to assumed locations of relays within the fault in the geological volume; 
 generating a three dimensional relay grid of relay sub-cells in the place of each relay cell set, the relay sub-cells of each relay grid being representative of a relay structure within the geological fault and having a finer grid-cell dimension than that of the cells of the relay cell set; 
 determining transmissibilities between the relay sub-cells; 
 determining transmissibilities between the relay cell sets based on the determined transmissibilities between the relay sub-cells, and 
 determining transmissibilities between the base cells based on the determined transmissibilities between the relay sub-cells; and wherein:
 the vertical faces of the fault cells are vertically offset from the fault; and 
 the fault cells comprise cutted fault cells and non-cutted fault cells, the cutted fault cells having a reduced height as compared to the height of the non-cutted fault cells, the method further comprising: 
 
 detecting hybrid-interface fault cells interfacing with both the fault and the cutted cells; 
 generating pseudo fault cells representing the fault cells in which the hybrid-interface fault cells are represented by pseudo fault cells having a height limited to the height of the portion of the hybrid-interface fault cells interfacing with the fault; and 
 the one or more sets of cells classified as relay cell sets are pseudo fault cells.

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